Impact of circulation on export production, dissolved organic matter, and dissolved oxygen in the ocean: Results from Phase II of the Ocean Carbon-cycle Model Intercomparison Project (OCMIP-2)

International audience Results are presented of export production, dissolved organic matter (DOM) and dissolved oxygen simulated by 12 global ocean models participating in the second phase of the Ocean Carbon-cycle Model Intercomparison Project. A common, simple biogeochemical model is utilized in d...

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Published in:Global Biogeochemical Cycles
Main Authors: Najjar, R., Jin, X., Louanchi, F., Aumont, O., Caldeira, K., Doney, S., Dutay, J.-C., Follows, M., Gruber, N., Joos, F., Lindsay, K., Maier-Reimer, E., Matear, R., Matsumoto, K., Monfray, P., Mouchet, A., Orr, J., Plattner, G.-K., Sarmiento, J., Schlitzer, R., Slater, R., Weirig, M.-F., Yamanaka, Y., Yool, A.
Other Authors: PennState Meteorology Department, Pennsylvania State University (Penn State), Penn State System-Penn State System, Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ), Modélisation du climat (CLIM), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2007
Subjects:
Online Access:https://hal.archives-ouvertes.fr/hal-03096840
https://hal.archives-ouvertes.fr/hal-03096840/document
https://hal.archives-ouvertes.fr/hal-03096840/file/2006GB002857.pdf
https://doi.org/10.1029/2006GB002857
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record_format openpolar
institution Open Polar
collection Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe)
op_collection_id ftccsdartic
language English
topic [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
spellingShingle [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
Najjar, R.
Jin, X.
Louanchi, F.
Aumont, O.
Caldeira, K.
Doney, S.
Dutay, J.-C.
Follows, M.
Gruber, N.
Joos, F.
Lindsay, K.
Maier-Reimer, E.
Matear, R.
Matsumoto, K.
Monfray, P.
Mouchet, A.
Orr, J.
Plattner, G.-K.
Sarmiento, J.
Schlitzer, R.
Slater, R.
Weirig, M.-F.
Yamanaka, Y.
Yool, A.
Impact of circulation on export production, dissolved organic matter, and dissolved oxygen in the ocean: Results from Phase II of the Ocean Carbon-cycle Model Intercomparison Project (OCMIP-2)
topic_facet [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
description International audience Results are presented of export production, dissolved organic matter (DOM) and dissolved oxygen simulated by 12 global ocean models participating in the second phase of the Ocean Carbon-cycle Model Intercomparison Project. A common, simple biogeochemical model is utilized in different coarse-resolution ocean circulation models. The model mean (±1s) downward flux of organic matter across 75 m depth is 17 ± 6 Pg C yr À1. Model means of globally averaged particle export, the fraction of total export in dissolved form, surface semilabile dissolved organic carbon (DOC), and seasonal net outgassing (SNO) of oxygen are in good agreement with observation-based estimates, but particle export and surface DOC are too high in the tropics. There is a high sensitivity of the results to circulation, as evidenced by (1) the correlation of surface DOC and export with circulation metrics, including chlorofluorocarbon inventory and deep-ocean radiocarbon, (2) very large intermodel differences in Southern Ocean export, and (3) greater export production, fraction of export as DOM, and SNO in models with explicit mixed layer physics. However, deep-ocean oxygen, which varies widely among the models, is poorly correlated with other model indices. Cross-model means of several biogeochemical metrics show better agreement with observation-based estimates when restricted to those models that best simulate deep-ocean radiocarbon. Overall, the results emphasize the importance of physical processes in marine biogeochemical modeling and suggest that the development of circulation models can be accelerated by evaluating them with marine biogeochemical metrics.
author2 PennState Meteorology Department
Pennsylvania State University (Penn State)
Penn State System-Penn State System
Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE)
Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)
Modélisation du climat (CLIM)
Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)
format Article in Journal/Newspaper
author Najjar, R.
Jin, X.
Louanchi, F.
Aumont, O.
Caldeira, K.
Doney, S.
Dutay, J.-C.
Follows, M.
Gruber, N.
Joos, F.
Lindsay, K.
Maier-Reimer, E.
Matear, R.
Matsumoto, K.
Monfray, P.
Mouchet, A.
Orr, J.
Plattner, G.-K.
Sarmiento, J.
Schlitzer, R.
Slater, R.
Weirig, M.-F.
Yamanaka, Y.
Yool, A.
author_facet Najjar, R.
Jin, X.
Louanchi, F.
Aumont, O.
Caldeira, K.
Doney, S.
Dutay, J.-C.
Follows, M.
Gruber, N.
Joos, F.
Lindsay, K.
Maier-Reimer, E.
Matear, R.
Matsumoto, K.
Monfray, P.
Mouchet, A.
Orr, J.
Plattner, G.-K.
Sarmiento, J.
Schlitzer, R.
Slater, R.
Weirig, M.-F.
Yamanaka, Y.
Yool, A.
author_sort Najjar, R.
title Impact of circulation on export production, dissolved organic matter, and dissolved oxygen in the ocean: Results from Phase II of the Ocean Carbon-cycle Model Intercomparison Project (OCMIP-2)
title_short Impact of circulation on export production, dissolved organic matter, and dissolved oxygen in the ocean: Results from Phase II of the Ocean Carbon-cycle Model Intercomparison Project (OCMIP-2)
title_full Impact of circulation on export production, dissolved organic matter, and dissolved oxygen in the ocean: Results from Phase II of the Ocean Carbon-cycle Model Intercomparison Project (OCMIP-2)
title_fullStr Impact of circulation on export production, dissolved organic matter, and dissolved oxygen in the ocean: Results from Phase II of the Ocean Carbon-cycle Model Intercomparison Project (OCMIP-2)
title_full_unstemmed Impact of circulation on export production, dissolved organic matter, and dissolved oxygen in the ocean: Results from Phase II of the Ocean Carbon-cycle Model Intercomparison Project (OCMIP-2)
title_sort impact of circulation on export production, dissolved organic matter, and dissolved oxygen in the ocean: results from phase ii of the ocean carbon-cycle model intercomparison project (ocmip-2)
publisher HAL CCSD
publishDate 2007
url https://hal.archives-ouvertes.fr/hal-03096840
https://hal.archives-ouvertes.fr/hal-03096840/document
https://hal.archives-ouvertes.fr/hal-03096840/file/2006GB002857.pdf
https://doi.org/10.1029/2006GB002857
geographic Southern Ocean
geographic_facet Southern Ocean
genre Southern Ocean
genre_facet Southern Ocean
op_source ISSN: 0886-6236
EISSN: 1944-8224
Global Biogeochemical Cycles
https://hal.archives-ouvertes.fr/hal-03096840
Global Biogeochemical Cycles, American Geophysical Union, 2007, 21 (3), pp.n/a-n/a. ⟨10.1029/2006GB002857⟩
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container_title Global Biogeochemical Cycles
container_volume 21
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spelling ftccsdartic:oai:HAL:hal-03096840v1 2023-05-15T18:25:46+02:00 Impact of circulation on export production, dissolved organic matter, and dissolved oxygen in the ocean: Results from Phase II of the Ocean Carbon-cycle Model Intercomparison Project (OCMIP-2) Najjar, R. Jin, X. Louanchi, F. Aumont, O. Caldeira, K. Doney, S. Dutay, J.-C. Follows, M. Gruber, N. Joos, F. Lindsay, K. Maier-Reimer, E. Matear, R. Matsumoto, K. Monfray, P. Mouchet, A. Orr, J. Plattner, G.-K. Sarmiento, J. Schlitzer, R. Slater, R. Weirig, M.-F. Yamanaka, Y. Yool, A. PennState Meteorology Department Pennsylvania State University (Penn State) Penn State System-Penn State System Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ) Modélisation du climat (CLIM) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ) 2007-09 https://hal.archives-ouvertes.fr/hal-03096840 https://hal.archives-ouvertes.fr/hal-03096840/document https://hal.archives-ouvertes.fr/hal-03096840/file/2006GB002857.pdf https://doi.org/10.1029/2006GB002857 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1029/2006GB002857 hal-03096840 https://hal.archives-ouvertes.fr/hal-03096840 https://hal.archives-ouvertes.fr/hal-03096840/document https://hal.archives-ouvertes.fr/hal-03096840/file/2006GB002857.pdf doi:10.1029/2006GB002857 info:eu-repo/semantics/OpenAccess ISSN: 0886-6236 EISSN: 1944-8224 Global Biogeochemical Cycles https://hal.archives-ouvertes.fr/hal-03096840 Global Biogeochemical Cycles, American Geophysical Union, 2007, 21 (3), pp.n/a-n/a. ⟨10.1029/2006GB002857⟩ [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment info:eu-repo/semantics/article Journal articles 2007 ftccsdartic https://doi.org/10.1029/2006GB002857 2021-12-19T00:35:49Z International audience Results are presented of export production, dissolved organic matter (DOM) and dissolved oxygen simulated by 12 global ocean models participating in the second phase of the Ocean Carbon-cycle Model Intercomparison Project. A common, simple biogeochemical model is utilized in different coarse-resolution ocean circulation models. The model mean (±1s) downward flux of organic matter across 75 m depth is 17 ± 6 Pg C yr À1. Model means of globally averaged particle export, the fraction of total export in dissolved form, surface semilabile dissolved organic carbon (DOC), and seasonal net outgassing (SNO) of oxygen are in good agreement with observation-based estimates, but particle export and surface DOC are too high in the tropics. There is a high sensitivity of the results to circulation, as evidenced by (1) the correlation of surface DOC and export with circulation metrics, including chlorofluorocarbon inventory and deep-ocean radiocarbon, (2) very large intermodel differences in Southern Ocean export, and (3) greater export production, fraction of export as DOM, and SNO in models with explicit mixed layer physics. However, deep-ocean oxygen, which varies widely among the models, is poorly correlated with other model indices. Cross-model means of several biogeochemical metrics show better agreement with observation-based estimates when restricted to those models that best simulate deep-ocean radiocarbon. Overall, the results emphasize the importance of physical processes in marine biogeochemical modeling and suggest that the development of circulation models can be accelerated by evaluating them with marine biogeochemical metrics. Article in Journal/Newspaper Southern Ocean Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Southern Ocean Global Biogeochemical Cycles 21 3 n/a n/a